全新世以来太行山前倾斜平原地下水演化规律 |
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关键词:Holocene groundwater recharge period evolution of hydrologic cycle piedmont clinoplain of Taihang mountains |
基金项目:河海大学博士后基金课题,国土资源部重点基础项目(9501110 ),国土资源部百名科技人才基金资助课题 |
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摘要: |
The Evolution Regularity of Groundwater in Piedmont Clinoplain of Taihang Mountains since Holocene |
The formation and the evolution of regional groundwater have been closely related to periodic hydrological cycle in piedmont clinoplain of Taihang mountains since Holocene.The main recharge period of groundwater was 8.0 to 3.5 ka B.P.,during which the recharge of groundwater was sufficient.This lay the foundation of present groundwater system. |
ZHANG Huang-hui,FEI Yu-hong,NIE Zhen-long,LI Hui-di.2000.The Evolution Regularity of Groundwater in Piedmont Clinoplain of Taihang Mountains since Holocene[J].Acta Geoscientica Sinica,21(2):121-127. |
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